Skip to main content

Advertisement

Log in

Temperature sensitivity of greenhouse gas production in wetland soils of different vegetation

  • Published:
Biogeochemistry Aims and scope Submit manuscript

Abstract

Organic matter decomposition regulates rates of carbon loss (CO2 and CH4) in wetlands and has implications for carbon sequestration in the context of changing global temperature. Here we determined the influence of temperature and vegetation type on both aerobic and anaerobic decomposition of organic matter in subtropical wetland soils. As in many other studies, increased temperature resulted in higher rates of respiration and methanogenesis under both aerobic and anaerobic conditions, and the positive effect of temperature depended on vegetation (source of carbon substrate to soil). Under anaerobic incubations, the proportion of gaseous C (CO2 and CH4) lost as CH4 increased with temperature indicating a greater sensitivity of methanogenesis to temperature. This was further supported by a wider range of Q10 values (1.4–3.6) for methane production as compared with anaerobic CO2 (1.3–2.5) or aerobic CO2 (1.4–2.1) production. The increasing strength of positive linear correlation between CO2:CH4 ratio and the soil organic matter ligno-cellulose index at higher temperature indicated that the temperature sensitivity of methanogenesis was likely the result of increased C availability at higher temperature. This information adds to our basic understanding of decomposition in warmer subtropical and tropical wetland systems and has implications for C models in wetlands with different vegetation types.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5

Similar content being viewed by others

References

  • Andersen JM (1976) An ignition method for determination of total phosphorus in lake sediments. Water Res 10:329–331

    Article  Google Scholar 

  • Arnold J, Corre MD, Veldkamp E (2008) Cold storage and laboratory incubation of intact soil cores do not reflect in situ nitrogen cycling rates of tropical forest soils. Soil Biol Biochem 40:2480–2483

    Article  Google Scholar 

  • Bardgett RD, Freeman C, Ostle NJ (2008) Microbial contributions to climate change through carbon cycle feedbacks. ISME J 2:805–814

    Article  Google Scholar 

  • Bartlett KB, Harriss RC (1993) Review and assessment of methane emissions from wetlands. Chemosphere 26:261–320

    Article  Google Scholar 

  • Bergman I, Klarqvist M, Nilsson M (2000) Seasonal variation in rates of methane production from peat of various botanical origins: effects of temperature and substrate quality. FEMS Microbiol Ecol 33:181–189

    Article  Google Scholar 

  • Bosatta E, Agren GI (1999) Soil organic matter quality interpreted thermodynamically. Soil Biol Biochem 31:1889–1891

    Article  Google Scholar 

  • Bridgham SD, Richardson CJ (1992) Mechanisms controlling soil respiration (CO2 and CH4) in southern peatlands. Soil Biol Biochem 24:1089–1099

    Article  Google Scholar 

  • Bridgham SD, Updegraff K, Pastor J (1998) Carbon, nitrogen, and phosphorus mineralization in northern wetlands. Ecology 79:1545–1561

    Article  Google Scholar 

  • Cadisch G, Giller KE (eds) (1997) Driven by nature. Plant litter quality and decomposition. CAB International, Wallingford, p 409

    Google Scholar 

  • Cao MK, Gregson K, Marshall S (1998) Global methane emission from wetlands and its sensitivity to climate change. Atmos Environ 32:3293–3299

    Article  Google Scholar 

  • IPCC (Intergovernmental Panel on Climate Change) (2007) Climate change 2007: the physical science basis. In: Solomon S, Qin D, Manning M et al. (eds) Contribution of working group I to the fourth assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge, UK

  • Chanton JP, Whiting GJ, Happell JD, Gerard G (1993) Contrasting rates and diurnal patterns of methane emission from emergent aquatic macrophytes. Aquat Bot 46:111–128

    Article  Google Scholar 

  • Chin KJ, Conrad R (1995) Intermediary metabolism in methanogenic paddy soil and the influence of temperature. FEMS Microbiol Ecol 18:85–102

    Article  Google Scholar 

  • Chin KJ, Lukow T, Conrad R (1999) Effect of temperature on structure and function of the methanogenic archaeal community in an anoxic rice field soil. Appl Environ Microbiol 65:2341–2349

    Google Scholar 

  • Conen F, Leifeld J, Seth B, Alewell C (2006) Warming mineralizes young and old soil carbon equally. Biogeosciences 3:515–519

    Article  Google Scholar 

  • Corstanje R, Reddy KR (2004) Response of biogeochemical indicators to a drawdown and subsequent reflood. J Environ Qual 33:2357–2366

    Article  Google Scholar 

  • DeBusk WF, Reddy KR (1998) Turnover of detrital organic carbon in a nutrient-impacted Everglades marsh. Soil Sci Soc Am J 62:1460–1468

    Article  Google Scholar 

  • Debusk WF, Reddy KR (2005) Litter decomposition and nutrient dynamics in a phosphorus enriched Everglades marsh. Biogeochemistry 75:217–240

    Article  Google Scholar 

  • Fang C, Moncrieff JB (2001) The dependence of soil CO2 efflux on temperature. Soil Biol Biochem 33:155–165

    Article  Google Scholar 

  • Fierer N, Craine JM, Mclauchlan K, Schimel JP (2005) Litter quality and the temperature sensitivity of decomposition. Ecology 86:320–326

    Article  Google Scholar 

  • Fierer N, Colman BP, Schimel JP, Jackson RB (2006) Predicting the temperature dependence of microbial respiration in soil: a continental-scale analysis. Global Biogeochem Cycles 20:GB3026

    Article  Google Scholar 

  • Fissore C, Giardina CP, Kolka RK, Trettin CC (2009) Soil organic carbon quality in forested mineral wetlands at different mean annual temperature. Soil Biol Biochem 41:458–466

    Article  Google Scholar 

  • Freeman C, Liska G, Ostle NJ, Jones SE, Lock MA (1995) The use of fluorogenic substrates for measuring enzyme-activity in peatlands. Plant Soil 175:147–152

    Article  Google Scholar 

  • Freeman C, Evans CD, Monteith DT, Reynolds B, Fenner N (2001) Export of organic carbon from peat soils. Nature 412:785

    Article  Google Scholar 

  • Freeman C, Fenner N, Ostle NJ et al (2004) Export of dissolved organic carbon from peatlands under elevated carbon dioxide levels. Nature 430:195–198

    Article  Google Scholar 

  • Fung I, John J, Lerner J, Matthews E, Prather M, Steele LP, Fraser PJ (1991) 3-Dimensional model synthesis of the global methane cycle. J Geophys Res 96:13033–13065

    Article  Google Scholar 

  • Grand M, Gaidos E (2010) Methane emission from a tropical Wetland in Ka’au Crater, O’ahu. Hawai’I Pacific Sci 64:57–72

    Article  Google Scholar 

  • Hein R, Crutzen PJ, Heimann M (1997) An inverse modeling approach to investigate the global atmospheric methane cycle. Global Biogeochem Cycles 11:43–76

    Article  Google Scholar 

  • Hines ME, Duddleston KN, Rooney-Varga JN, Fields D, Chanton JP (2008) Uncoupling of acetate degradation from methane formation in Alaskan wetlands: connections to vegetation distribution. Global Biogeochem Cycles 22:2017

    Article  Google Scholar 

  • Hogg EH, Lieffers VJ, Wein RW (1992) Potential carbon losses from peat profiles—effects of temperature, drought cycles, and fire. Ecol Appl 2:298–306

    Article  Google Scholar 

  • Ipsilantis I, Sylvia DM (2007) Abundance of fungi and bacteria in a nutrient impacted Florida wetland. Appl Soil Ecol 35:272–280

    Article  Google Scholar 

  • King GM, Berman T, Wiebe WJ (1981) Methane formation in the acidic peats of Okefenokee Swamp, Georgia. Am Midl Nat 105:386–389

    Article  Google Scholar 

  • Klinger LF, Zimmerman PR, Greenberg JP, Heidt LE, Guenther AB (1994) Carbon trace gas fluxes along a successional gradient in the Hudson-Bay lowland. J Geophys Res 99:1469–1494

    Article  Google Scholar 

  • Knoblauch C, Zimmermann U, Blumenberg M, Michaelis W, Pfeiffer EM (2008) Methane turnover and temperature response of methane-oxidizing bacteria in permafrost-affected soils of northeast Siberia. Soil Biol Biochem 40:3004–3013

    Article  Google Scholar 

  • Larionova AA, Zolotareva BN, Yevdokimov IV, Sapronov DV, Kuzyakov YV, Buegger F (2008) The rates of organic matter renewal in gray forest soils and chernozems. Eur Soil Sci 41:1378–1386

    Article  Google Scholar 

  • Leifeld J, Fuhrer J (2005) The temperature response of CO2 production from bulk soils and soil fractions is related to soil organic matter quality. Biogeochemistry 75:433–453

    Article  Google Scholar 

  • Liski J, Ilvesniemi H, Makela A, Westman CJ (2000) Temperature dependence of old soil organic matter. Ambio 29:56–57

    Google Scholar 

  • Lloyd J, Taylor JA (1994) On the temperature-dependence of soil respiration. Func Ecol 8:315–323

    Article  Google Scholar 

  • Lovley DR, Klug MJ (1983) Sulfate reducers can out-compete methanogens at fresh-water sulfate concentrations. Appl Environ Microbiol 45:187–192

    Google Scholar 

  • Matthews E, Fung I (1987) Methane emission from natural wetlands: global distribution, area and environmental characteristics of sources. Global Biogeochem Cycles 1:61–86

    Article  Google Scholar 

  • McKenzie C, Schiff S, Aravena R, Kelly C, St. Louis V (1998) Effect of temperature on production of CH4 and CO2 from Peat in a Natural and Flooded Boreal Forest Wetland. Clim Change 40:247–266

    Article  Google Scholar 

  • McLatchey GP, Reddy KR (1998) Regulation of organic matter decomposition and nutrient release in a wetland soil. J Environ Qual 27:1268–1274

    Article  Google Scholar 

  • McNamara NP, Plant T, Oakley S, Ostle NJ (2008) Gully hotspot contribution to landscape methane and carbon dioxide fluxes in a northern peatland. Sci Total Environ 404:354–360

    Article  Google Scholar 

  • Melillo JM, Aber JD, Linkins AE, Ricca A, Fry B, Nadelhoffer KJ (1989) Carbon and nitrogen dynamics along the decay continuum—plant litter to soil organic-matter. Plant Soil 115:189–198

    Article  Google Scholar 

  • Mitra S, Wassmann R, Vlek PLG (2005) An appraisal of global wetland area and its carbon stock. Curr Sci 88:25–34

    Google Scholar 

  • Moore TR, Dalva M (1993) The influence of temperature and water table position on carbon dioxide and methane emissions from laboratory columns of peatland soils. J Soil Sci 44:651–664

    Article  Google Scholar 

  • Moore TR, Dalva M (1997) Methane and carbon dioxide exchange potentials of peat soils in aerobic and anaerobic laboratory incubations. Soil Biol Biochem 29:1157–1164

    Article  Google Scholar 

  • Morrissey LA, Livingston GP (1992) Methane emissions from Alaska Arctic tundra: an assessment of local spatial variability. J Geophy Res 97:16661–16670

    Article  Google Scholar 

  • Page SE, Rieley JO, Banks CJ (2010) Global and regional importance of the tropical peatland carbon pool. Global Change Biol. doi:10.1111/j.1365-2486.2010.02279.x

  • Phelps TJ, Zeikus JG (1985) Effect of fall turnover on terminal carbon metabolism in Lake Mendota sediments. Appl Environ Microbiol 50:1285–1291

    Google Scholar 

  • Raich JW, Schlesinger WH (1992) The global carbon dioxide flux in soil respiration and its relationship to vegetation and climate. Tellus 44:81–99

    Google Scholar 

  • Reddy R, DeLaune RD (2008) Biogeochemistry of wetlands: science and applications. Taylor and Francis group LLC, Boca Raton

    Book  Google Scholar 

  • Reichstein M, Subke J-A, Angeli AC, Tenhunen JD (2005) Does the temperature sensitivity of decomposition of soil organic matter depend upon water content, soil horizon, or incubation time? Global Change Biol 11:1754–1767

    Article  Google Scholar 

  • Rey A, Jarvis P (2006) Modelling the effect of temperature on carbon mineralization rates across a network of European forest sites (FORCAST). Global Change Biol 12:1894–1908

    Article  Google Scholar 

  • Rooney-Varga JN, Giewat MW, Duddleston KN, Chanton JP, Hines ME (2007) Links between archaeal community structure, vegetation type and methanogenic pathway in Alaskan peatlands. FEMS Microbiol Ecol 60:240–251

    Article  Google Scholar 

  • Rowland AP, Roberts JD (1994) Lignin and cellulose fractionation in decomposition studies using acid-detergent fiber methods. Commun Soil Sci Plant Anal 25:269–277

    Article  Google Scholar 

  • Scanlon D, Moore T (2000) Carbon dioxide production from peatland soil profiles: the influence of temperature, oxic/anoxic conditions and substrate. Soil Sci 165:153–160

    Article  Google Scholar 

  • Schipper LA, Reddy KR (1994) Methane production and emissions from four reclaimed and Pristine Wetlands of Southeastern United States. Soil Sci Soc Am J 58:1270–1275

    Article  Google Scholar 

  • Segers R (1998) Methane production and methane consumption: a review of processes underlying wetland methane fluxes. Biogeochemistry 41:23–51

    Article  Google Scholar 

  • Seo M (2002) Influence of nutrients, vegetation types and seasonality on microbial activities of carbon in a subtropical wetland, Masters Thesis. University of Florida, Gainesville, FL

  • Shaver GR, Giblin AE, Nadelhoffer KJ, Thieler KK, Downs MR, Laundre JA, Rastetter EB (2006) Carbon turnover in Alaskan tundra soils: effects of organic matter quality, temperature, moisture and fertilizer. J Ecol 94:740–753

    Article  Google Scholar 

  • Shindell DT, Faluvegi G, Koch DM, Schmidt GA, Unger N, Bauer SE (2009) Improved attribution of climate forcing to emissions. Science 326:716–718

    Article  Google Scholar 

  • Smemo KA, Yavitt JB (2006) A multi-year perspective on methane cycling in a shallow peat fen in central New York State, USA. Wetlands 26:20–29

    Article  Google Scholar 

  • Strom L, Mastepanov M, Christensen TR (2005) Species-specific effects of vascular plants on carbon turnover and methane emissions from wetlands. Biogeochemistry 75:65–82

    Article  Google Scholar 

  • Teh YA, Silver WL (2006) Effects of soil structure destruction on methane production and carbon partitioning between methanogenic pathways in tropical rain forest soils. J Geophyl Res-Biogeo, 111, G01003, 1–8. doi:10.1029/2005JG000020

  • Updegraff K, Pastor J, Bridgham SD, Johnston CA (1995) Environmental and substrate controls over carbon and nitrogen mineralization in northern wetlands. Ecol Appl 5:151–163

    Article  Google Scholar 

  • USEPA (1993) Methods for chemical analysis of water and wastes. Environmental Monitoring Support Lab, Cincinnati, OH

    Google Scholar 

  • Valentine DW, Holland EA, Schimel DS (1994) Ecosystem and physiological controls over methane production in northern wetlands. J Geophys Res 99:1563–1571

    Article  Google Scholar 

  • Goering HK, Van Soest, PJ (1970). Forage fiber analysis (apparatus, reagents, procedures and some applications). In: Agriculture Handbook No. 379. Agriculture Research Service, United States Department of Agriculture, Washington, USA

  • Whiting GJ, Chanton JP (1993) Primary production control of methane emission from wetlands. Nature 364:794–795

    Article  Google Scholar 

  • Wickland KP, Neff JC (2008) Decomposition of soil organic matter from boreal black spruce forest: environmental and chemical controls. Biogeochemistry 87:29–47

    Article  Google Scholar 

  • Winkler JP, Cherry RS, Schlesinger WH (1996) The Q10 relationship of microbial respiration in a temperate forest soil. Soil Biol Biochem 28:1067–1072

    Article  Google Scholar 

  • Wright AL, Reddy KR (2001) Heterotrophic microbial activity in northern Everglades wetland soils. Soil Sci Soc Am J 65:1856–1864

    Article  Google Scholar 

  • Yavitt JB, Lang GE (1990) Methane production in contrasting wetland sites: response to organic-chemical components of peat and to sulfate reduction. Geomicrobiol J 8:27–46

    Article  Google Scholar 

  • Yavitt JB, Williams CJ, Wieder RK (1997) Production of methane and carbon dioxide in peatland ecosystems across North America: effects of temperature, aeration, and organic chemistry of peat. Geomicrobiol J 14:299–316

    Article  Google Scholar 

  • Zak DR, Holmes WE, MacDonald NW, Pregitzer KS (1999) Soil temperature, matric potential, and the kinetics of microbial respiration and nitrogen mineralization. Soil Sci Soc Am J 63:575–584

    Article  Google Scholar 

Download references

Acknowledgments

This work was supported by funding from the St Johns River water management district, Palatka, Florida. We sincerely appreciate the critical reviews provided by the anonymous reviewers, which greatly improved the overall quality of our paper.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to K. S. Inglett.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Inglett, K.S., Inglett, P.W., Reddy, K.R. et al. Temperature sensitivity of greenhouse gas production in wetland soils of different vegetation. Biogeochemistry 108, 77–90 (2012). https://doi.org/10.1007/s10533-011-9573-3

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10533-011-9573-3

Keywords

Navigation